Assessment of Water Resources Mixing in Karstic Aquifers: A Case Study of Garu Karstic Springs, East of Khuzestan

Authors

1 Department of Geology, Faculty of Earth Scinces, Shahid Chamran University of Ahvaz

2 Department of Geology, Faculty of Earth Sciences, Shahid Chamran University of Ahvaz

Abstract

     Mixing is one of the most important factors in the altering of the groundwater quality. The presence of various components in the Zagros zone such as oil brine, waters affected by evaporative formations such as Gachsaran has caused the mixing process to play a fundamental role in the quality of these water resources. Garu Spring in the Masjed Soleiman area can be used as an indicator to investigating the mechanism of groundwater resources mixing in the Zagros zone. Most of the Asmari anticline groundwater discharged by this spring, unfortunately, due to mixing with saline water in the northwest of Asmari anticline, quality of this huge resource of fresh water has reduced. In this research, we tried to investigate the mixing of fresh and saline water using hydrochemical studies and hydrogeochemical combination diagrams and methods. Chemical analysis of the main elements of the 20 samples and TOC of the 10 samples of groundwater was investigated. Br/Cl ratio and Combination diagrams, which have obvious linear trend between the sodium and chlorine, shows that fresh and saline water are mixed. Also, TOC values indicate contamination of Garu saline spring by organic substances. Phreeqc software results to determine the percentage of the area, Shows that salinity of karstic aquifer of Asmari anticline and Garu springs have several reasons, including dissolution of evaporative Gachsaran formation and oilfield brine in the area. The main reason for salinity in the wet season is an influx of high volume Temby river water, and in the dry season is mixing with oil brines.
 

Keywords


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